摘要
潜水含水层是地下水资源中与人类活动和生物圈联系最为紧密的一部分,对潜水的研究一直是水文地质工作的主要内容之一。综合利用电阻率测深法(电测深法)、高密度电阻率法(高密度电法)和激发极化法(激电法)进行潜层地下水的探测,对这些方法的实测数据进行反演,对比分析了不同电探方法与含水层空间位置的对应关系。研究结果表明:三种电探方法都能够较好地圈定潜水层的基本范围,其中测深法和激电法的勘探结果更加精确,而高密度电法对地层的刻画更直观。
Phreatic aquifer is one of the most closely associated groundwater resources with human′s activities and the biosphere,and has long been the focus of hydrogeologists.Vertical resistivity sounding(VRS),high density resistivity(HDR)and induced polarization(IP)methods are combined to investigate phreatic water.Results from those methods are analyzed to locate phreatic aquifer after electrical data reversion from VRS,HDR and IP.The results show that electrical methods can achieve good effect to depict basic aquifer location.The VRS and IP show more accurate than the other two methods,however,HDR is more workable visually.
作者
张建锋
李贺领
余能成
杨志杰
张俊杰
刘红蕾
占士军
程岁泉
汪雪萍
智春生
ZHANG Jianfeng;LI Heling;YU Nengcheng;YANG Zhijie;ZHANG Junjie;LIU Honglei;ZHAN Shijun;CHENG Suiquan;WANG Xueping;ZHI Chunsheng(College of Resources and Environment,Henan University of Engineering,Zhengzhou 451191,China)
出处
《河南工程学院学报（自然科学版）》
2020年第1期24-28,共5页
Journal of Henan University of Engineering：Natural Science Edition
基金
河南工程学院博士基金(D2012004)
郑州市科技发展计划项目(131PPTGG414-7)。
关键词
潜水含水层
电阻率测深
高密度电法
激发极化
phreatic aquifer
vertical resistivity sounding
high density resistivity
induced polarization
